mode ................................................... 14
5 Errors associated with SURFEX .................................................................... 15
6 Statistical correction of model results .............................................................. 19
7 Original and corrected 2-m air temperature .................................................... 22
8 Original and corrected 10-m
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
recorded at 5-13 km depth, but fewer than
yesterday.
GPS deformation: Measurements from around Eyjafjallajökull indicate no major net
discplaceaments, suggesting a stabilization of the surface deformation
since yesterday.
Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64
km distance from the eruption site shows that about 5 % of the ash is
smaller
/media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf
opportunity evaluation
Case studies
NOE Net
SEAS-NVE
Findings of case studies
• Distribution companies generally well
equipped for climate change
– Cabling of all overhead lines well under way
– Distribution boxes in areas with increased risk of
flooding are elevated already
– Salt spray further inland is becoming an increasing
problem for substations and transformers
Cabling in Denmark
/media/ces/James-Smith_Edward_CES_2010.pdf
in the data used in making the
decision and the factors are interlinked, all of which makes
the problem highly complex. The part of the net defined by
variables and links is relatively easily communicated to
stakeholders (Henriksen et al., 2007b). However the
tal Management 88 (2008) 1025–1036
quantitative part, with the conditional probability tables
(CPTs), the numbers, is the step where
/media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
glacier, and a general land rise
along the southern coast and in the countries interior (figure 1). This rise results from recent melt
of the Icelandic glaciers, which have been melting since the late 19th century. An acceleration in
land uplift is even evident in the Southeast. STL analysis of vertical GPS measurements in 1997-
2015 from Höfn in Hornafjörður show over 8 mm/yr uplift in the first
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
construction and maintenance.
7. Path dependency, meaning that roads will likely continue to exist even if the
underlying need for them decreases.
8. Social shifts, personal ownership of cars no longer seen as necessary. Car-sharing
becomes part of a suite of mobility options within the collective transportation
system.
9. Behavioral shifts, mobility no longer dominant variable in daily life
/media/loftslag/Group4.pdf
............................................................................................................... 8
PAST AND PRESENT CHANGES IN CLIMATE AND HYDROLOGY
Dyrrdal, A.V., Vikhamar-Schuler, D., Stranden, H.B. and Skaugen, T.
Analysis of past snow conditions in Norway – Time periods 1931-60, 1961-90 and 1979-08 ............................. 10
Crochet, P.
Impacts of historic climate variations on streamflow characteristics in Icelandic rivers
/media/ces/ces-oslo2010_proceedings.pdf
lying areas in the City is illustrated for present climate in Figure 5. It is
expected that the future water level of the Horsens fiord will increase by 1 meter by the end of this
century.
Station 270045: Upstream Lake Nørrestrand
0
0.5
1
1.5
2
2.5
3
3.5
4
1 2 3 4 5 6 7 8 9 10 11 12
Month
M
ea
n
d
is
ch
ar
g
e
(m
3 /
s)
Present: Mean A2: Mean
Station 280001: Upstream Bygholm Lake
0
1
2
3
4
5
6
/media/loftslag/Horsens_case.pdf
increase that will affect existing facilities. It will affect the most important
touristic destinations of the country [7]. South-eastern Spain hosts some of the most
popular destinations for tourists from the UK and other European countries. According
to the IPCC [8], Spain could lose 40% of its German tourists and up to 100% of its
British tourists. Hein [5] estimates that climate change
/media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf